12 research outputs found
Cascading Crises: Society in the Age of COVID-19
The tsunami of change triggered by the COVID-19 pandemic has transformed society in a series of cascading crises. Unlike disasters that are more temporarily and spatially bounded, the pandemic has continued to expand across time and space for over a year, leaving an unusually broad range of second-order and third-order harms in its wake. Globally, the unusual conditions of the pandemicâunlike other crisesâhave impacted almost every facet of our lives. The pandemic has deepened existing inequalities and created new vulnerabilities related to social isolation, incarceration, involuntary exclusion from the labor market, diminished economic opportunity, life-and-death risk in the workplace, and a host of emergent digital, emotional, and economic divides. In tandem, many less advantaged individuals and groups have suffered disproportionate hardship related to the pandemic in the form of fear and anxiety, exposure to misinformation, and the effects of the politicization of the crisis. Many of these phenomena will have a long tail that we are only beginning to understand. Nonetheless, the research also offers evidence of resilience on several fronts including nimble organizational response, emergent communication practices, spontaneous solidarity, and the power of hope. While we do not know what the post COVID-19 world will look like, the scholarship here tells us that the virus has not exhausted societyâs adaptive potential
Cascading Crises: Society in the Age of COVID-19
The tsunami of change triggered by the COVID-19 pandemic has transformed society in a series of cascading crises. Unlike disasters that are more temporarily and spatially bounded, the pandemic has continued to expand across time and space for over a year, leaving an unusually broad range of second-order and third-order harms in its wake. Globally, the unusual conditions of the pandemicâunlike other crisesâhave impacted almost every facet of our lives. The pandemic has deepened existing inequalities and created new vulnerabilities related to social isolation, incarceration, involuntary exclusion from the labor market, diminished economic opportunity, life-and-death risk in the workplace, and a host of emergent digital, emotional, and economic divides. In tandem, many less advantaged individuals and groups have suffered disproportionate hardship related to the pandemic in the form of fear and anxiety, exposure to misinformation, and the effects of the politicization of the crisis. Many of these phenomena will have a long tail that we are only beginning to understand. Nonetheless, the research also offers evidence of resilience on several fronts including nimble organizational response, emergent communication practices, spontaneous solidarity, and the power of hope. While we do not know what the post COVID-19 world will look like, the scholarship here tells us that the virus has not exhausted societyâs adaptive potential
Rapid response seismic networks in Europe: lessons learnt from the L'Aquila earthquake emergency
The largest dataset ever recorded during a normal fault seismic sequence was acquired during the 2009 seismic emergency triggered by the damaging earthquake in L'Aquila (Italy). This was possible through the coordination of different rapid-response seismic networks in Italy, France and Germany. A seismic network of more than 60 stations recorded up to 70,000 earthquakes. Here, we describe the different open-data archives where it is possible to find this unique set of data for studies related to hazard, seismotectonics and earthquake physics. Moreover, we briefly describe some immediate and direct applications of emergency seismic networks. At the same time, we note the absence of communication platforms between the different European networks. Rapid-response networks need to agree on common strategies for network operations. Hopefully, over the next few years, the European Rapid-Response Seismic Network will became a reality
Rapid response seismic networks in Europe: lessons learnt from the L'Aquila earthquake emergency
<p>The largest dataset ever recorded during a normal fault seismic sequence was acquired during the 2009 seismic emergency triggered by the damaging earthquake in L'Aquila (Italy). This was possible through the coordination of different rapid-response seismic networks in Italy, France and Germany. A seismic network of more than 60 stations recorded up to 70,000 earthquakes. Here, we describe the different open-data archives where it is possible to find this unique set of data for studies related to hazard, seismotectonics and earthquake physics. Moreover, we briefly describe some immediate and direct applications of emergency seismic networks. At the same time, we note the absence of communication platforms between the different European networks. Rapid-response networks need to agree on common strategies for network operations. Hopefully, over the next few years, the European Rapid-Response Seismic Network will became a reality.</p>
Rapid response seismic networks in Europe : lessons learnt from the L'Aquila earthquake emergency
The largest dataset ever recorded during a normal fault seismic sequence was acquired during the 2009 seismic emergency triggered by the damaging earthquake in L'Aquila (Italy). This was possible through the coordination of different rapid-response seismic networks in Italy, France and Germany. A seismic network of more than 60 stations recorded up to 70,000 earthquakes. Here, we describe the different open-data archives where it is possible to find this unique set of data for studies related to hazard, seismotectonics and earthquake physics. Moreover, we briefly describe some immediate and direct applications of emergency seismic networks. At the same time, we note the absence of communication platforms between the different European networks. Rapid-response networks need to agree on common strategies for network operations. Hopefully, over the next few years, the European Rapid-Response Seismic Network will became a reality
Rapid response to the earthquake emergency of May 2012 in the Po Plain, northern Italy
International audienceRapid-response seismic networks are an important element in the response to seismic crises. They temporarily improve the detection performance of permanent monitoring systems during seismic sequences. The improvement in earthquake detection and location capabilities can be important for decision makers to assess the current situation, and can provide invaluable data for scientific studies related to hazard, tectonics and earthquake physics. Aftershocks and the clustering of the locations of seismic events help to characterize the dimensions of the causative fault. Knowing the number, size and timing of the aftershocks or the clustering seismic events can help in the foreseeing of the characteristics of future seismic sequences in the same tectonic environment. Instrumental rapid response requires a high degree of preparedness. A mission in response to a magnitude (Ml) 6 event with a rupture length of a few tens of kilometers might involve the deployment within hours to days of 30-50 seismic stations in the middle of a disaster area of some hundreds of square kilometers, and the installation of an operational center to help in the logistics and communications. When an earthquake strikes in a populated area, which is almost always the case in Italy, driving the relevant seismic response is more difficult
Rapid response to the earthquake emergency of May 2012 in the Po Plain, northern Italy
Rapid-response seismic networks are an important element
in the response to seismic crises. They temporarily improve
the detection performance of permanent monitoring
systems during seismic sequences. The improvement in earthquake
detection and location capabilities can be important for
decision makers to assess the current situation, and can provide
invaluable data for scientific studies related to hazard, tectonics
and earthquake physics. Aftershocks and the clustering
of the locations of seismic events help to characterize the dimensions
of the causative fault. Knowing the number, size and
timing of the aftershocks or the clustering seismic events can
help in the foreseeing of the characteristics of future seismic
sequences in the same tectonic environment.
Instrumental rapid response requires a high degree of
preparedness. A mission in response to a magnitude (ML) 6
event with a rupture length of a few tens of kilometers
might involve the deployment within hours to days of 30-50
seismic stations in the middle of a disaster area of some hundreds
of square kilometers, and the installation of an operational
center to help in the logistics and communications.
When an earthquake strikes in a populated area, which is almost
always the case in Italy, driving the relevant seismic response
is more difficult. Temporary station sites are chosen
such as to optimize the network geometry for earthquake
locations and source study purposes. Stations have to be installed
in quiet, but easily reachable, sites, and for real-time
data transmission, the sites might need to have optical intervisibility.
The operational center can remain in a town if
there is one within the damaged area, and it should coordinate
the actions of the field teams and provide information
to colleagues, the Civil Protection Authorities and the general
public. The emergency system should operate as long
as the seismic rate remains high; the duration of any mission
might also depend on the seismic history of the area involved.
This study describes the seismic response following
the May 20, 2012, ML 5.9 earthquake in northern Italy, which
included rapid deployment of seismological stations in the
field for real-time seismic monitoring purposes, the coordination
of further instrumental set-ups according to the spatial
evolution of the seismic sequence, and data archiving